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气候时期
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  climatic periods
     Using linear method of equal and Fokker - Planck equation, the nonlinear open function treatment different climatic periods to a simple stochastic climate model is discussed in the paper. The probability density and the output functions of the ice age, the glacial age and the contemporary age have been got.
     本文利用等效线性化法和Fokker-planck方程,对一个简单的非线性随机模式非线性项在不同气候时期的参数化进行了讨论,得到了冰期、间冰期和现代气候的概率分布密度及输出响应特征。
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     The content of titanium, representing the relative abundance of terrestrial detritus, changes significantly during different climatic periods. In details, the highest Ti contents occurred during Stage 4, also higher during Stage 2 and the late Stage 3, indicating larger terrestrial fluxes.
     结果表明,代表碎屑物质的量的Ti含量在不同气候时期变化明显,其中在氧同位素第4期碎屑比例最大,第2期和第3期末期,碎屑所占比例也较高,代表较大的碎屑输入通量。
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  “气候时期”译为未确定词的双语例句
     the climatic environment again became warm and wet at 4.97-2.50 ka , during which limnic peat was developed at 3.44-2.50 ka;
     4.97~2.50kaB.P. 为暖湿气候时期,其间3.44~2.50kaB.P.
短句来源
     (3) Climate conditions in the Last Glacial Maximum (LGM, 18 kaBP) were remarkably different from the present.
     (3) 末次冰盛期(18kaBP)是两万年来距人类环境最近、与现代反差最大的气候时期
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     whereas the move of SiO2 and the gather of stable constant elements A1203, Fe2O3+FeO, Mn, TiO hi fluvio-lacustrine facies and palaeosols is related to the biochemistry weathering during warm-humid climate, hi the 38 sedimentary cycles, the contents of non-stable K2O, MgO, CaO, Na2O hi the fluvio-lacustrine facies are usually higher than those in the aeolian sands, it shows that during warm-humid climate, precipitation is abundant, the earth's surface around is drenched and washed out, so them can be assembled to the special close lowland.
     在这38个沉积旋迥中,非稳定性元素K_2O、MgO、CaO、Na_2O通常在河湖相中的含量也较风成砂高,这说明,暖湿气候时期由于降水较丰,四周地表受到淋滤和流水冲刷作用,才使之能够汇集于本区这种特殊的比较封闭的低地。
短句来源
     And it is concluded that the aeolian sands and loess are the sediments in the dry-cold period.
     风成沙和黄土是晚更新世以来相对干冷气候时期沉积的。
短句来源
     (3) The drab -red stratum lay at 3. 7m below ground level about the Baiquesi area in the eastern foot of the Diancangshan Mountains is deposited about 122. 18ha B. P. (ESR dating) which reveals it takes form in a damp-hot stage representing deep sea oxygan isotopes (5e).
     (3)点苍山东侧白雀寺地区深3.7m处的褐红色地展形成的ESR年龄为12218KaBP,揭示出该地层形成于深海氧同位素5e阶段所代表的一个温热气候时期
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  相似匹配句对
     Now, climate of the whole world is being unstable.
     目前,全球气候正处于不稳定的时期
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     A Historical Re-investigation of Climatic Conditions during the West and East Han Dynasties
     两汉时期气候状况的历史学再考察
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     Atmosphere and Climate
     大气层和气候
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     ,dry—cold climate;
     ,气候干冷 ;
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     Romance in SARS Period
     SARS时期的爱情
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  climatic periods
The high-resolution sequences probably represent alternating, relatively wet and dry climatic periods, with a periodicity of about 100 000 years.
      
The period of 1550 AD to 1850 AD is interrupted by two relatively arid and cold climatic periods: one was from 1630 AD to 1700 AD and another was 1750 AD to 1820 AD.
      
In addition, several of the climatic periods and especially local human influence can be proved by the geomorphological findings.
      
Five climatic periods have been identified: a Subatlantic Cold Period (>amp;lt;150 b.c.), cold and arid; the Roman Warm Period (150 b.c.-a.d.
      
Land-ice teleconnections of cold climatic periods during the last Glacial/Interglacial transition
      
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It is attempet to understand the climaic changes and the sedimentary environment since the Quaternary Period in Sjara-Osol-Gol District by studying the element distribution in the Quaternary strata at Disiaogou Bay of the Sjara-Osol-Gol River at southeast edge of Mu Us Sandy Land. It is pointed out that there occurred three -warm-wet periods and three dry-cold periods ince the Later Pleistocene period and the aeolian sands and loess were accu mulated during relevant dry-cold climate since the Later Pleistocene...

It is attempet to understand the climaic changes and the sedimentary environment since the Quaternary Period in Sjara-Osol-Gol District by studying the element distribution in the Quaternary strata at Disiaogou Bay of the Sjara-Osol-Gol River at southeast edge of Mu Us Sandy Land. It is pointed out that there occurred three -warm-wet periods and three dry-cold periods ince the Later Pleistocene period and the aeolian sands and loess were accu mulated during relevant dry-cold climate since the Later Pleistocene period. And it is concluded that the aeolian sands and loess are the sediments in the dry-cold period.

本文试图通过研究萨拉乌苏河滴哨沟湾第四纪地层中的元素分布,认识该地区第四纪以来气候的变迁与沉积环境。文中指出滴哨沟湾地区晚更新世以来存在三个暖湿期和三个干冷期。风成沙和黄土是晚更新世以来相对干冷气候时期沉积的。

Since Teihert (1958) and Chave (1967) pointed out that some places where a lot of shallow water sediments contained over 50% carbonate were located in some higher latitude areas, a few scholars have observed that both cold water carbonate and warm water carbonate exist in the world, especially in some higher latitude areas , and this fact has clarified a wrong idea, which is popular among some geologists , that all carbonate rocks can be explained by the " temperate climate" model. But in China, there is hardly...

Since Teihert (1958) and Chave (1967) pointed out that some places where a lot of shallow water sediments contained over 50% carbonate were located in some higher latitude areas, a few scholars have observed that both cold water carbonate and warm water carbonate exist in the world, especially in some higher latitude areas , and this fact has clarified a wrong idea, which is popular among some geologists , that all carbonate rocks can be explained by the " temperate climate" model. But in China, there is hardly any report about cold water carbonate sediments of lakes.

本文以草海两个钻孔剖面的孢粉资料为佐证,讨论了该区晚上新世晚期以来不同气候条件下形成的沉积物中,CaCO_3等作古气候指示剂的可能性。研究表明:在大陆湖盆沉积区与溶蚀区(物源区)相距不远、沉积区没有远源物质加入的情况下,寒冷气候时期,沉积盆地的堆积物中CaCO_3的含量较高;而温暖气候时期沉积物中的CaCO_3含量较低。

The present paper had deal with as follow problems:Ⅰ Ever since mid-peroid of holocene,The climatic changes are as the following: Moist-hot climatic——Temperate climatie——Dry-cool climatie;Ⅱ Ever since mid-peroid of holocene,the changes of vegetation are as following: Forest with subtropical floral element——Temperate deciduous broadleaf forest——Forest steppe(northern part)and temperate deciduous broadleaf ferost(southern part);Ⅲ When we think about the building program on the loess plateau of northern part in...

The present paper had deal with as follow problems:Ⅰ Ever since mid-peroid of holocene,The climatic changes are as the following: Moist-hot climatic——Temperate climatie——Dry-cool climatie;Ⅱ Ever since mid-peroid of holocene,the changes of vegetation are as following: Forest with subtropical floral element——Temperate deciduous broadleaf forest——Forest steppe(northern part)and temperate deciduous broadleaf ferost(southern part);Ⅲ When we think about the building program on the loess plateau of northern part in shaanxi province,not only attend to that the change of ecotope are coused by mankind activities but also thank about influence of climatic change ever since mid-peroid of holocene.

本文主要论述了以下几点:(1)自全新世中期以业的气候变化:暖湿气候时期——干凉气候时期;(2)自全新世中期以来的植被变化,具亚热带成分的阔叶林——落叶阔叶林——森林草原(北部)和落叶阔叶林(南部);(3)考虑陕北黄土高原的建设方针时,不但要注意人类活动所引起生态环境的变化,也要考虑自全新世中期以来气候变化的影响。

 
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